Typical glacial landscapes T Parson – Allerton Grange School.

Slides:



Advertisements
Similar presentations
Glaciers Chapter 8, Section 2.
Advertisements

Glaciers Carve Land and Move Sediments
The Glacial History of Michigan
Jeopardy GlaciersLandforms More Landforms RANDOM Q $100 Q $200 Q $300 Q $400 Q $500 Q $100 Q $200 Q $300 Q $400 Q $500 Final Jeopardy.
By: Ryan Alex Scott Whit Louie
Glaciers Chapter 15.1.
In the Beginning… Ice Age: period of time when freezing temperatures created ice sheets across continents. Glaciers covered most of.
The Ice Age and Last Glacial Maximum (LGM) Lesson 4 Starter Slides.
The Last Glacial Maximum (LGM)
Snow line – where snow remains year round. Formation of Glacial Ice from Snow.
Glacial Processes and Landforms. What is a glacier? How do glaciers form?
Glacial and Periglacial Landforms. Rivers of Ice Glacial Processes Glacial Landforms Periglacial Landscapes The Pleistocene Ice Age Epoch Deciphering.
The Last Glacial Maximum (LGM) Lesson 1 Starter Slides on the nature and timing of the LGM.
Charity I. Mulig.
Ice Ages glacials The common term for the periods when there were major cold phases known as glacials, and ice sheets covered large areas of the world.
7.1 Glaciers.
Chapter 7: Erosion and Deposition
Formation  Snow accumulation  More winter snowfall than summer melt  Glacier formation is similar to sedimentary rock formation.
Lecture 24: Survey of the Last Glacial Maximum Part IV, p ; Chapter 12 (p )
GLACIERS AND LANDFORMATION
Glaciers Topics: Types of Glaciers Glacier Movement Deposits by Glaciers The Ice Age Glaciers and Global Warming Glacial Rebound.
Glaciation. "What causes ice sheets to expand and contract? Are the present ice sheets growing or shrinking? How will global warming impact the ice sheets?
Glaciers. Glaciers are massive streams of ice flowing down across the landscape. Gravity pulls them downward and their weight causes them to move, ever.
Unit 1: Chapter 1 Test Review
GLACIAL ENVIRONMENTS 4 Periglacial processes and landforms: permafrost
Glacial Processes and Landforms What is a glacier? How do glaciers form?
Ch. 5 Glaciers & Ice Ages p guided notes.
LEARNING GOALS 1. I AM LEARNING THE IMPACT OF HUMAN ACTIVITIES AND TECHNOLOGIES ON WATER RESOURCES 2. I AM INVESTIGATING THE FACTORS THAT AFFECT LOCAL.
Earth Science: 7.1A Glaciers. Glaciers  As recently as 15,000 years ago, up to 30 percent of earth’s land was covered by an glacial ice.  Earth was.
Landforms and Landscapes of Continental Glaciation.
World Geography Unit 1: Land and Water Forms Glaciers as Agents of Erosion.
Glaciers October 21st, Pre - Activity Knowledge Check on the note sheet provided, answer the true or false questions.
GLACIATION About 15 million square kilometres of the earth’s surface are currently covered with glaciers.
Chapter 18: Glaciers. Introduction Glacier: thick mass of ice that originates on land from the accumulations, compaction and recrystallization of snow.
CLIMATE CHANGE THE GREAT DEBATE Session 3. Advancing Franz Josef Glacier in 1996, New Zealand.
GLACIERS A glacier is: Any large mass of ice that moves slowly over land Any large mass of ice that moves slowly over land.
Connecticut’s Glacial History
Glacial Modification of Terrain
Glaciers and Ice Ages By: Liz Alessi Brittany Spalding Megan Timmers.
Glaciers & Erosion. Glaciers: What are they? very powerful agent of erosion mass of moving ice How are glaciers formed? when snow and ice accumulate to.
Glaciers.  Glaciers: Masses of ice built up over thousands of years.  Alpine Glaciers: Glaciers that occur in high altitudes, such as mountains.  Continental.
Masses of Ice that: 1)Are at least 100 m thick 2)Originate on land 3)Move How Glaciers Form.
Chapter 17 Glacial and Periglacial Processes and Landforms
Glaciers & Glaciation GLG Physical Geology Bob Leighty.
UNIT 8 Surface processes Biology and Geology 3. Secondary Education TYPES OF GLACIERS.
Glacial Processes and Landforms
G LACIERS M INI U NIT Types, Formation and Effects.
Tuesday March 8, 2011 (Types of Glaciers; Formation of Glaciers)
Glaciers.  Glaciers: Masses of ice built up over thousands of years.  Alpine Glaciers: Glaciers that occur in high altitudes, such as mountains.  Continental.
Glaciers and Ice Ages By: Briana Brandt and Lindsey Kosinski.
Study Guide Chapter What is a glacier? 2.Distinguish between alpine and continental glaciation. 3.Explain how a glacier moves. Explain how a crevass.
Chapter 7.3 Glaciers. Glacier Any large mass of ice that moves slowly over land. Two kinds: – Continental Glaciers – Valley Glaciers.
Chapter 17 Glaciers.
Years before present This graph shows climate change over the more recent 20,000 years. It shows temperature increase and atmospheric carbon dioxide. Is.
Glaciation CGC1P. What is a Glacier? Glaciers are made up of fallen snow that, over many years, compresses into large, thickened ice masses Glacier don’t.
AS Geography Cold Environments. True or False? 1. 20,000 years ago a third of the land surface of the earth was covered by snow and ice – this included.
Glaciers. Formation of glaciers Glaciers – a large mass of moving ice. At high elevations and in polar regions, snow can remain on the ground year-round.
Chapter 17-Glaciers Section 1: Glaciers – Moving Ice
Chapter 18 Glaciers & Glaciation
Ice on the Land How has climate change affected the distribution of ice around the globe?
An agent of erosion, weathering, and deposition
By: Briana Brandt and Lindsey Kosinski
Glacial Processes and Landforms
Cold & High Altitude Environments
Bell Ringer What is a Sherpa?
Glacial Processes and Landforms
Chapter 21.
Glacial Erosion.
DO FIRST A _____________ is a stream that empties into another stream.
Glaciers.
Presentation transcript:

Typical glacial landscapes T Parson – Allerton Grange School

Location Cold Environments You need to know details on the following… Glacial environments Periglacial environments Alpine regions What, where and characteristics.

Task : Location of glacial environments Using the next slide and answering in at least 3 sentences describe the location of : Glacial environments Periglacial environments Alpine regions What, where and characteristics.

Location Cold Environments Glacial Alpine Tundra

Snow line – Describe why there is a snow line?

Task : KEY TERMS Try to define the following… Fluvioglacial (glacifluvial) Glacier Ice ages Ice sheet Periglacial Tundra

KEY TERMS revealed FLUVIOGLACIAL (GLACIFLUVIAL) Processes and landforms associated with the action of glacial meltwater GLACIER A tongue shaped mass of ice moving slowly down a valley ICE AGES The common term for the period when there were major cold phases known as glacials, and ice sheets covered large areas of the world. The last ice age lasted from about 2 million years ago to BP (before present) known as the Quaternary glaciation. At this time 30% of the Earths surface was covered in ice compared to 10% today.

KEY TERMS revealed ICE SHEET A body of ice covering an area of at least km2.Today, ice sheets cover Antarctica and Greenland, with smaller sheets (ice caps) covering areas of Iceland, Spitsbergen and Norway. Major ice sheets can be up to 2,000m thick today; those that occurred at the maximum extent of the quaternary glaciation could have been up to twice that thickness. PERIGLACIAL Processes and landforms associated with the fringe of, or the area near to, an ice sheet or glacier

KEY TERMS revealed TUNDRA A climatic and vegetation type found in the most northerly parts of Eurasia and North America. Tundra- like environments also occur above the tree line in mountainous areas such as the Alps, Rockies, Andes and Himalayas. Quaternary tundra climate affected Central N America and Europe, tundra today covers around 25% of the earths surface. Tundra

Drag and drop slide / / - glacier p1 0/ / - picture p5 sse/ / sse/ / - Tundra p9